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Driefand, Ahmed, Schiffman, Peter (2004) Very low-temperature alteration of sideromelane in hyaloclastites and hyalotuffs from Kilauea and Mauna Kea volcanoes: implications for the mechanism of palagonite formation. clays and clay minerals, 52 (5) 622-634 doi:10.1346/ccmn.2004.0520508

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Reference TypeJournal (article/letter/editorial)
TitleVery low-temperature alteration of sideromelane in hyaloclastites and hyalotuffs from Kilauea and Mauna Kea volcanoes: implications for the mechanism of palagonite formation
Journalclays and clay minerals
AuthorsDriefand, AhmedAuthor
Schiffman, PeterAuthor
Year2004 (October 1)Volume52
Page(s)622-634Issue5
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1346/ccmn.2004.0520508Search in ResearchGate
Mindat Ref. ID147934Long-form Identifiermindat:1:5:147934:2
GUID18a58d89-6642-457f-bc2a-91d580402d27
Full ReferenceDriefand, Ahmed, Schiffman, Peter (2004) Very low-temperature alteration of sideromelane in hyaloclastites and hyalotuffs from Kilauea and Mauna Kea volcanoes: implications for the mechanism of palagonite formation. clays and clay minerals, 52 (5) 622-634 doi:10.1346/ccmn.2004.0520508
Plain TextDriefand, Ahmed, Schiffman, Peter (2004) Very low-temperature alteration of sideromelane in hyaloclastites and hyalotuffs from Kilauea and Mauna Kea volcanoes: implications for the mechanism of palagonite formation. clays and clay minerals, 52 (5) 622-634 doi:10.1346/ccmn.2004.0520508
In(2004, October) clays and clay minerals Vol. 52 (5) Springer Science and Business Media LLC


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